古今文献和地图上的多瑙河及其河口地区和海岸线(三角洲)。

P. Gâștescu
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引用次数: 0

摘要

古今文献和地图上的多瑙河及其河口地区和海岸线(三角洲)。从古代至今的文件和地图上都有多瑙河口的记载。特别是多瑙河河口及其三角洲,许多古典学者(希罗多德、埃拉托斯提尼、波利布斯、托勒密、斯特拉波等)和最近的科学研究人员都对这个话题感兴趣,他们把注意力集中在多瑙河支流的数量和三角洲王国从形成到现在的演变上。19世纪下半叶,在多瑙河欧洲委员会的支持下,哈特利爵士的地图出版了。该地图的目的是为了帮助选择和修正一个臂的工程,以方便海上航行。在20世纪,i . vidra(1909-1911)、国家水资源委员会(1964)和地理研究所(1983)印制了其他几张地图。此外,还制作了一系列罗马尼亚领土的地形图。这一区域是积聚过程的结果,南北海岸的海流,移动的河流冲积物阻塞了河口,形成了多瑙河三角洲和Halmyris泻湖,整个形成了Razim Sinoie湖群。由于河流冲积物的贡献,这一海洋海岸部分的特点通常是海洋空间的扩大,但目前的条件(多瑙河沉积物体积的减少、海洋小海侵和人为干预(苏利纳支流和米迪亚角河口的大坝)导致一些地区的海岸线退缩。为了确定前进和后退的部分,并设定相应的年速率,使用了150多年的现有地形图系列、30年的水文测量和1975年开始的一系列卫星图像。
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The Danube River and its mouths area and coast line (delta) in documents and maps from the ancient times to the present.
The Danube River and its mouths area and coast line (delta) in documents and maps from the ancient times to the present. The Danube mouth as reported in documents and maps from the Antiquity to date.This mouth of the Danube and its Delta in particular, where a topic interest for many classical scholars (Herodotus, Erathostenes, Polybus, Ptolemey, Strabo etc) and recent scientific researchers who focused their attention on the number of Danube arms and the evolution of the Delta realm from the moment of its formation to the present configuration. The second half of the 19th century witnessed the publication of Sir Ch. Hartley’s map under the aegis of the Danube European Commission. The map was intended to help the selection of and correction works to one the arms in order to facilitate maritime navigation on it. Several other maps were printed in the 20th century by I.Vidraşcu, 1909-1911, the State Water Committee, 1964 and the Institute of Geography, 1983. In addition a series of topographical maps of Romania territory have also been produced. This sector was created as a result of accumulation processes, the north-south coastal marine currents, moving the river alluvia blocked the river mouth forming the Danube Delta and Halmyris lagoon, the whole becoming Razim Sinoie Lake Complex. This marine shore sector, due to the contribution of river alluvia, is characterized generally by the advance in the marine space, but the current conditions (reducing the volume of sediments from the Danube, marine minitransgression and anthropogenic interventions (by the dams raised at the mouth of the Sulina branch and Cape Midia) generate shoreline retreat in some areas. To identify portions of advancement and retreat, and setting the corresponding annual rates, existing topographic map series for a period of over 150 years, hydrographic measurements for 30 years and series of satellite images starting from 1975 were used.
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